Soil Data Explorer - PARKE

Official Series Description

Lab Data Summary

Aggregate lab data for the PARKE soil series. This aggregation is based on all pedons with a current taxon name of PARKE, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to PARKE were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
113	85IL121049	1985IL121049	Parke	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7516972,-88.9543
113	85IL191015	1985IL191015	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.2781083,-88.2324611
113	86IL193017	1986IL193017	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.2156,-88.1859194
113	83P0569	83IL049013	Parke	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1308327,-88.5233307
113	87P0155	86IL051098	Parke	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9072227,-89.2163925
114A	PM7687	1976IN133087	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.5237833,-86.9358972
114A	CL7740	1977IN021040	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.4654167,-86.9425722
114A	GN7926	1979IN055026	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1024944,-87.2229306
114B	DC7805	1978IN031005	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2663528,-85.33065
114B	JN7805	1978IN071005	Parke	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8856917,-85.9062194
114B	JF7921	1979IN077021	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8061944,-85.6729444
114B	80IL145024	1980IL145024	Parke	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.0533863,-89.3748935
120B	MT8005	1980IN101005	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.643325,-86.8510667
n/a	CO-005	1955-OH029-005	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-007	1955-OH141-007	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-008	1955-OH141-008	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-024	1956-OH029-024	Parke	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WA-006	1958-OH165-006	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WA-013	1958-OH165-013	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	HA-001	1977-OH061-001	Parke	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	85IL191016	1985IL191016	Parke	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PARKE soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the PARKE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the PARKE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the PARKE series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

There are insufficient data to create the 3D mountains figure.

Competing Series

Soil series competing with PARKE share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the PARKE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the PARKE series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

There are insufficient data to create the 3D mountains figure.

Soil series sharing subgroup-level classification with PARKE, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database (updated 2024-10-23).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. IL-2010-09-09-07 | Wayne County -

   Typical pattern of soils and parent material in the Parke-Negley association (Soil Survey of Wayne County, Illinois).

2. IN-2010-09-24-13 | Owen County -

   Typical pattern of soils and parent materials in the Parke-Pike-Gallimore association (Soil Survey of Owen County, Indiana).

Map Units

Map units containing PARKE as a major component. Limited to 250 records.

Map Unit Name	Symbol	Map Unit Area (ac)	Map Unit Key	National Map Unit Symbol	Soil Survey Area	Publication Date	Map Scale
Parke silt loam, 5 to 12 percent slopes, eroded	15C2	2200	173844	5tww	il005	1981	1:12000
Parke silt loam, 2 to 5 percent slopes	15B	595	173443	2zczq	il049	1986	1:15840
Parke silt loam, 5 to 10 percent slopes, eroded	15C2	200	173444	2zxcc	il049	1986	1:15840
Parke silt loam, 2 to 5 percent slopes	15B	7852	173379	2zczq	il051	1991	1:15840
Parke silt loam, 5 to 10 percent slopes, eroded	15C2	5674	173380	2zxcc	il051	1991	1:15840
Parke silt loam, 10 to 15 percent slopes, eroded	15D2	2307	173381	5tdy	il051	1991	1:15840
Parke silty clay loam, 10 to 18 percent slopes, severely eroded	15D3	1003	806873	w2m5	il055	2005	1:12000
Parke silt loam, 2 to 5 percent slopes, eroded	15B2	268	2027529	2zxcb	il121	2008	1:12000
Parke silt loam, 5 to 10 percent slopes, eroded	15C2	544	1721552	2zxcc	il135	2007	1:12000
Parke silt loam, 10 to 18 percent slopes, eroded	15D2	148	1721529	1vsd6	il135	2007	1:12000
Parke silt loam, 5 to 10 percent slopes, eroded	15C2	3708	178999	2zxcc	il173	1990	1:15840
Parke silt loam, 10 to 15 percent slopes, eroded	15D2	787	179000	6086	il173	1990	1:15840
Parke silt loam, 5 to 10 percent slopes, eroded	15C2	2229	2024919	2zxcc	il191	2008	1:12000
Parke silt loam, 2 to 5 percent slopes, eroded	15B2	852	2024918	2zxcb	il191	2008	1:12000
Parke silt loam, 5 to 10 percent slopes, eroded	15C2	719	1543859	2zxcc	il193	2006	1:12000
Parke silt loam, 10 to 18 percent slopes, eroded	15D2	254	1543860	1nthy	il193	2006	1:12000
Parke silt loam, 2 to 5 percent slopes	15B	201	1543858	2zczq	il193	2006	1:12000
Parke silt loam, 12 to 18 percent slopes, eroded	PaD2	460	159621	5c32	in021	1980	1:15840
Parke silt loam, 12 to 18 percent slopes, eroded	PaD2	1000	162968	5gl1	in027	1969	1:20000
Parke silt loam, 2 to 6 percent slopes, eroded	PaB2	912	162965	5gky	in027	1969	1:20000
Parke silt loam, 6 to 12 percent slopes, severely eroded	PaC3	832	162967	5gl0	in027	1969	1:20000
Parke silt loam, 6 to 12 percent slopes, eroded	PaC2	470	162966	5gkz	in027	1969	1:20000
Parke silt loam, 6 to 12 percent slopes, eroded	PaC2	1218	535643	kzct	in037	1978	1:15840
Parke silt loam, 2 to 6 percent slopes	PaB	929	535642	kzcs	in037	1978	1:15840
Parke silt loam, 12 to 18 percent slopes, severely eroded	PaD3	928	535644	kzcv	in037	1978	1:15840
Alford-Parke silt loams, 18 to 50 percent slopes	AmF	953	160095	5clc	in051	1986	1:15840
Parke silt loam, 12 to 18 percent slopes, eroded	PbD2	1871	161563	5f3q	in055	1984	1:15840
Parke silt loam, 6 to 12 percent slopes, eroded	PbC2	1049	161562	5f3p	in055	1984	1:15840
Parke silt loam, 2 to 6 percent slopes, eroded	PbbB2	1230	1907092	220h3	in071	1985	1:15840
Parke silt loam, 6 to 12 percent slopes, eroded	PbbC2	939	1907093	220h4	in071	1985	1:15840
Urban land-Parke-Medora-Negley complex, 6 to 18 percent slopes	UlbC	52	1947795	23cv3	in071	1985	1:15840
Urban land-Parke-Medora complex, 2 to 6 percent slopes	UlaB	26	1947798	23cv6	in071	1985	1:15840
Parke silt loam, 6 to 12 percent slopes, eroded	PkC2	734	161683	5f7l	in081	1975	1:15840
Parke silt loam, 2 to 6 percent slopes, eroded	PkB2	557	161682	5f7k	in081	1975	1:15840
Parke silt loam, 6 to 12 percent slopes, eroded	PbbC2	411	1708154	1vbgr	in101	1984	1:15840
Parke silt loam, 12 to 18 percent slopes, eroded	PbbD2	370	1708155	1vbgs	in101	1984	1:15840
Parke silt loam, 6 to 12 percent slopes	PaC	721	535552	kz8w	in105	1979	1:15840
Parke-Chetwynd silt loams, 12 to 18 percent slopes	PcD	512	535553	kz8x	in105	1979	1:15840
Parke silt loam, 2 to 6 percent slopes	PaB	509	535551	kz8v	in105	1979	1:15840
Parke silt loam, 6 to 12 percent slopes, eroded	PkC2	3156	163237	5gvq	in109	1979	1:15840
Parke silt loam, 12 to 18 percent slopes	PkD	1681	163238	5gvr	in109	1979	1:15840
Parke silt loam, 6 to 12 percent slopes, eroded	PbbC2	3155	166215	5kys	in119	1997	1:12000
Parke silt loam, 6 to 12 percent slopes, severely eroded	PbbC3	953	166216	5kyt	in119	1997	1:12000
Parke silt loam, 12 to 18 percent slopes, eroded	PbbD2	849	166217	5kyv	in119	1997	1:12000
Parke silt loam, 12 to 18 percent slopes, severely eroded	PbbD3	761	166218	5kyw	in119	1997	1:12000
Parke silt loam, 5 to 8 percent slopes, moderately eroded	PaC2	355	159777	5c83	in121	1965	1:20000
Parke silt loam, 2 to 5 percent slopes	PaB	200	159776	5c82	in121	1965	1:20000
Parke silt loam, 8 to 15 percent slopes, moderately eroded	PaD2	152	159778	5c84	in121	1965	1:20000
Parke silt loam, 6 to 12 percent slopes, eroded	PeC2	1483	159850	5cbg	in133	1979	1:15840
Parke silt loam, 2 to 6 percent slopes, eroded	PeB2	989	159849	5cbf	in133	1979	1:15840
Parke silt loam, 6 to 12 percent slopes, eroded	PaC2	390	160744	5d89	in145	1968	1:15840
Parke silt loam, 2 to 6 percent slopes, eroded	PaB2	278	160743	5d88	in145	1968	1:15840
Parke silt loam, 12 to 18 percent slopes, severely eroded	PaD3	103	162699	5g9c	in153	1966	1:15840
Parke silt loam, 6 to 12 percent slopes, severely eroded	PaC3	70	162698	5g9b	in153	1966	1:15840
Parke silt loam, 12 to 18 percent slopes, eroded	PaD2	449	159684	5c53	in167	1971	1:20000
Parke silt loam, 2 to 6 percent slopes, eroded	PaB2	353	159683	5c52	in167	1971	1:20000
Parke silt loam, 2 to 6 percent slopes	PaB	450	537381	l15w	oh009	1981	1:15840
Urban land-Alfic Udarents-Parke complex, 0 to 12 percent slopes	UAPXC	497	2652887	2pyyz	oh061	1980	1:15840
Parke silt loam, 8 to 15 percent slopes, eroded	PbC2	339	169418	5p93	oh061	1980	1:15840
Parke silt loam, 3 to 8 percent slopes, eroded	PbB2	276	169417	5p92	oh061	1980	1:15840
Parke silt loam, 25 to 35 percent slopes	PbE	261	169420	5p95	oh061	1980	1:15840
Parke silt loam, 15 to 25 percent slopes	PbD	188	169419	5p94	oh061	1980	1:15840
Urban land-Alfic Udarents-Parke complex, 12 to 25 percent slopes	UAPXD	103	2652888	2qy7b	oh061	1980	1:15840
Urban land-Alfic Udarents-Parke complex, 25 to 50 percent slopes	UAPXF	47	2652889	2qy7c	oh061	1980	1:15840
Parke-Urban land complex, 8 to 15 percent slopes, eroded	PbUC2	26	3422043	31ggp	oh061	1980	1:15840
Parke-Urban land complex, 3 to 8 percent slopes, eroded	PbUB2	5	3422042	31ggn	oh061	1980	1:15840
Parke silt loam, 6 to 12 percent slopes, eroded	PaC2	2250	171068	5r0b	oh089	1986	1:15840
Parke silt loam, 0 to 3 percent slopes	PaA	639	537699	l1j4	oh131	1984	1:15840
Parke silt loam, 3 to 8 percent slopes	PaB	212	537700	l1j5	oh131	1984	1:15840
Parke silt loam, 2 to 6 percent slopes	PaB	174	171377	5rb9	oh165	1967	1:20000
Parke silt loam, 6 to 18 percent slopes, moderately eroded	PaD2	162	171378	5rbb	oh165	1967	1:20000
Parke-Urban land complex, 2 to 6 percent slopes	PaUB	27	3422294	31gjq	oh165	1967	1:20000

Map of Series Extent

Approximate geographic distribution of the PARKE soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry (updated 2024-10-30).